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Computation of clear-air radar backscatter from numerical simulations of turbulence: 2. Backscatter moments throughout the lifecycle of a Kelvin-Helmholtz instability

机译:从湍流的数值模拟中计算出晴空雷达的反向散射:2.在开尔文-亥姆霍兹不稳定性整个生命周期中的反向散射矩

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Franke et al. (2011) describe a numerical simulation of the instability and turbulent breakdown of Kelvin-Helmholtz (KH) billows at a high Reynolds number, numerical assessment of radar backscatter, and accuracies of inferred Doppler spectral moments for one test volume. Those results suggest a potential for significant measurement biases for radars that obtain backscatter from refractive index fluctuations. We present in this paper the morphology of computed radar moments throughout the KH instability lifecycle for two radar configurations in order to reveal the evolving character of radar backscatter and compare the radar velocity estimates with true velocities throughout the evolution, and to provide guidance, and cautions, for the interpretation of these dynamics in observational data. Results reveal strong variations in backscatter moments and character, and dependence on radar measurement parameters, that should be beneficial in the interpretation of such measurements in the atmosphere. Backscatter power predictions agree reasonably with observations of such events and their temporal evolutions. Our results also reveal a potential for significant measurement or sensitivity biases, some of which were predicted previously. Examples include a lack of significant backscatter power in well-mixed billow cores, suggesting possibly weak turbulence where in fact it may be strongest, maximum backscatter power in the billow exteriors, where refractive index fluctuations are large but turbulence is weak, underestimated vertical velocities within the KH billows at early times, and inferred significant vertical velocities where true vertical velocities are near zero at late stages of restratification, especially in the edge regions of the turbulence layer.
机译:弗兰克(Franke)等人。 (2011年)描述了在高雷诺数下开尔文-亥姆霍兹(KH)滚滚的不稳定性和湍流破裂的数值模拟,对雷达后向散射的数值评估,以及一个测试量的推断多普勒频谱矩的准确性。这些结果表明,对于从折射率波动中获得反向散射的雷达,可能存在较大的测量偏差。我们在本文中介绍两种雷达配置在整个KH不稳定性生命周期中计算出的雷达矩的形态,以揭示雷达反向散射的演变特征,并将雷达速度估计值与整个演化过程中的真实速度进行比较,并提供指导和注意事项,用于解释观测数据中的这些动态。结果表明,背向散射矩和特性的强烈变化以及对雷达测量参数的依赖性,这将有利于大气中此类测量的解释。背向散射功率预测与此类事件及其时间演变的观测结果合理地吻合。我们的结果还显示出潜在的重大测量或灵敏度偏差,其中一些是先前预测的。例子包括在充分混合的波涛芯中缺乏明显的反向散射能力,这表明湍流可能实际上较弱,而实际上波涛外部的反向散射能力最大,那里的折射率波动较大,但湍流较弱,内部垂直速度低估了KH在早期起伏,并推断出显着的垂直速度,在再平衡的后期,特别是在湍流层的边缘区域,真实的垂直速度接近于零。

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